•made up of rocks, and deep rock in mantle
•formed through geological process that is crystalline solid
•element and compound
silver, quartz, halites
reflective
dull
habit
luster
cleavage and fracture
hardness
color
streak
others
overall shape and growth
equant
elongate
platy
same lenght same shape
cube/ sphere
ex. garnet
prism like (pencil)
flattened and thin crystals
appearance with light reflection
metallic and non metallic
opoque(solid color) reflective
ex. gold and silver
dull, greasy and silky
ex. silicates
cleavage is the tendency of an object to be broken in smooth surface
fracture broken in random or irregular surface
resistance of scratching
1.talc
2.gypsum
3.calcite
4. fluorite
5.apatite
6. ortholite
7.quartz
8.topaz
9. corundum
10. diamond
obvious appearance
not reliable
powdered form
more reliable
some attach to hand magnet like magnetite
this parallel grooves
1.natural elements
2.silicates
3.oxides
4.sulfides
5.sulfates
6.halites
7.carbonates
8.phosphates
9. mineraloids
made of pure elements
ex. gold
silicon, oxygen, metals
ex. feldspar
oxygen, metals
ex. magnetite
sulfur, metals
ex. pyrite
mixture of metals
halogen, metals
ex. salt
carbon, oxygen, metals
ex. dolomite
phosphorus, oxygen
ex. apatite
if not fit to 8 properties
ex. amber
sedimentary
igneous
metamorphic
recyclers
they recycle old rocks to form new rocks
classic sedimentary rocks
chemical rocks
biochemical/organic
common rocks
ex. sand stone
generation
transportation
lithification
weathering
erosion
new rocks
evaporites (precipitated minerals)
ex.limestone
remains of living organisms
ex. coal/chalk
"ignis" fire
originated from cooled magma
volcanic
plutonic
magma rising to earth's surface
magma below earth's surface
basaltic magma
andesitic magma
rhyolitic magma
partial melting parts of atmosphere
partial melting of mantle rocks with water
melting of parts of continental crust
form from existing rocks
turn metamorphic when they are subjected to very high heat and pressure
process of changes in mineral
composition and texture that can occur in any solid
rocks
Changes can be due to increasing temperature
that are enough to promote chemical reaction and enough to cause melting
200 degree Celsius-1100 degree Celsius
a. Contact metamorphism
b. Regional metamorphism
Foliation is produced
when tabular minerals grow perpendicular to the
direction of pressure.
Changes due to
increase in temperature where rocks come
in contact with heat source (e.g. magma
chamber).